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Journal articles on the topic 'Mineralogy Mineralogy'

Author: Grafiati

Published: 4 June 2021

Last updated: 11 February 2022

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1

Hoppe, G. "Zur Geschichte der Geowissenschaften im Museum für Naturkunde zu Berlin Teil 4: Das Mineralogische Museum der Universität Berlin unter Christian Samuel Weiss von 1810 bis 1856." Fossil Record 4, no. 1 (January 1, 2001): 3–27. http://dx.doi.org/10.5194/fr-4-3-2001.

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Die Universitätsgründung in Berlin von 1810 war verbunden mit der Übernahme des Lehrbetriebes der aufgelösten Bergakademie, die nur noch in Form des Bergeleveninstituts bzw. Bergelevenklasse für die Finanzierung der Ausbildung der Bergeleven weiter bestand, sowie mit der Übernahme des von der Bergakademie genutzten Königlichen Mineralienkabinetts der preußischen Bergverwaltung als Mineralogisches Museum der Universität. Infolge des Todes von D. L. G. Karsten im Jahre 1810 erhielt der Leipziger Physiker und Mineraloge C. S. Weiss den Lehrstuhl für Mineralogie, den er bis zu seinem Tode 1856 innehatte. Weiss entwickelte die Lehre Werners, die die Mineralogie einschließlich Geologie umfasste, in kristallographischer Hinsicht weiter, während sich später neben ihm zwei seiner Schüler anderen Teilgebieten der Mineralogie annahmen, G. Rose der speziellen Mineralogie und E. Beyrich der geologischen Paläontologie. Der Ausbau der Sammlungen durch eigene Aufsammlungen, Schenkungen und Käufe konnte in starkem Maße fortgesetzt werden, auch zunehmend in paläontologischer Hinsicht, sodass das Mineralogische Museum für das ganze Spektrum der Lehre gut bestückt war. Der streitbare Charakter von Weiss verursachte zahlreiche Reibungspunkte. <br><br> History of the Geoscience Institutes of the Natural History Museum in Berlin. Part 4 <br><br> The establishment of the University in Berlin in 1810 resulted in the adoption of the teaching of the dissolved Bergakademie and of the royal Mineralienkabinett of the Prussian mining department, which was used by the Bergakademie before it became the Mineralogical Museum of the University. The Bergakademie continued to exist only as Bergeleveninstitut or Bergelevenklasse for financing the education of the mining students. The physicist and mineralogist C. S. Weiss was offered the chair of mineralogy after the death of D. L. G. Karsten 1810; he had the position to his death in 1856. Weiss developped the crystallographic part of the science of Werner which included mineralogy and geology. Two of his pupils progressed two other parts of mineralogy, G. Rose the speciel mineralogy and E. Beyrich the geological paleontology. The enlargement of the collections continued on large scale by own collecting, donations and purchases, also more paleontological objects, so that the Mineralogical Museum presented a good collection of the whole spectrum of the field. The pugnacious nature of Weiss resulted in many points of friction. <br><br> doi:<a href="http://dx.doi.org/10.1002/mmng.20010040102" target="_blank">10.1002/mmng.20010040102</a>

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2

Valsami-Jones, E., D. A. Polya, and K. Hudson-Edwards. "Environmental mineralogy, geochemistry and human health." Mineralogical Magazine 69, no. 5 (October 2005): 615–20. http://dx.doi.org/10.1180/s0026461x00045473.

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This issue of Mineralogical Magazine is the 5th in a loosely defined series of special thematic issues (or part issues), deriving from conferences organized by the Mineralogical Society. The associated conference was entitled ‘Environmental Mineralogy, Geochemistry and Human Health’ and took place in January 2005, in Bath. A common thread to all these Mineralogical Society conferences has been the role of mineralogy in applied science and technology and particularly in environmental science, focussing on the multidisciplinarity of modern mineralogy; the conferences (and special issues) have been particularly successful in bringing along scientists from outside traditional Mineralogy/Earth Sciences. Notably, the series comes at a time when the popularity of Mineralogy/Geology, but also science in general, is low, and many, particularly young, scientists are seeking to place themselves in a better position in the eye of the public and the media, and often also to find new focus for their research. A primary ambition for the series is thus to demonstrate Mineralogy's extensive outreach and has so far succeeded in giving the scientific community a sense of the wider role mineralogists can play.

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3

Graham, Shaun, and Nynke Keulen. "Nanoscale Automated Quantitative Mineralogy: A 200-nm Quantitative Mineralogy Assessment of Fault Gouge Using Mineralogic." Minerals 9, no. 11 (October 29, 2019): 665. http://dx.doi.org/10.3390/min9110665.

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Effective energy-dispersive X-ray spectroscopy analysis (EDX) with a scanning electron microscope of fine-grained materials (submicrometer scale) is hampered by the interaction volume of the primary electron beam, whose diameter usually is larger than the size of the grains to be analyzed. Therefore, mixed signals of the chemistry of individual grains are expected, and EDX is commonly not applied to such fine-grained material. However, by applying a low primary beam acceleration voltage, combined with a large aperture, and a dedicated mineral classification in the mineral library employed by the Zeiss Mineralogic software platform, mixed signals could be deconvoluted down to a size of 200 nm. In this way, EDX and automated quantitative mineralogy can be applied to investigations of submicrometer-sized grains. It is shown here that reliable quantitative mineralogy and grain size distribution assessment can be made based on an example of fault gouge with a heterogenous mineralogy collected from Ikkattup nunaa Island, southern West Greenland.

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4

Gutmann, J. "Mineralogy." Eos, Transactions American Geophysical Union 79, no. 27 (1998): 320. http://dx.doi.org/10.1029/98eo00242.

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5

Kokkaliari, Maria, and Ioannis Iliopoulos. "Application of Near-Infrared Spectroscopy for the identification of rock mineralogy from Kos Island, Aegean Sea, Greece." Bulletin of the Geological Society of Greece 55, no. 1 (January 3, 2020): 290. http://dx.doi.org/10.12681/bgsg.20708.

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Near-Infrared spectroscopy (NIR) is a useful tool for direct and on-site identification of rock mineralogy in spite of the difficulties arising in spectral evaluation, due to limited availability of spectral libraries at the time. Especially in the field, a functional methodology for the identification and evaluation if possible, of the geologic materials, is of interest to many researchers. However, several different parameters (such as grain size, color, mineralogy, texture, water content etc.) can affect the spectroscopic properties of the samples resulting in spectral variability. The subject of the present work focuses in various lithotypes (monzodiorite, diorite, altered diorite, actinolite schist, cataclasite, slate) from Kos Island, Aegean Sea, in Greece, all bearing hydrous minerals in various amounts. The evaluation of the results obtained from NIR spectroscopy offered important qualitative information about the mineralogy of the lithotypes examined. The important asset of the method is that no sample preparation was necessary. From the reflectance spectra, the NIR-active minerals that were identified include chlorite, micas, amphiboles and epidotes. Petrographic and mineralogic analyses were also employed in order to confirm the NIR results and provide more detailed information about the mineralogy of the samples, the grain size and the orientation of the minerals. Correlation of wavelength positions at ~1400 nm with loss on ignition (LOI) values led us to relate the various lithotypes in terms of their petrological affinities. NIR spectroscopy was proved to be a useful tool, especially for the mineralogic identification of rocks underwent low- to medium grade metamorphism, from greenschist to amphibolite facies.

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6

Naldrett, A. J. "Mineralogy is alive." European Journal of Mineralogy 12, no. 1 (February 7, 2000): 5–6. http://dx.doi.org/10.1127/ejm/12/1/0005.

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7

Dunham, A. C. "Developments in industrial mineralogy: II. Archaeological mineralogy." Proceedings of the Yorkshire Geological Society 49, no. 2 (November 1992): 105–15. http://dx.doi.org/10.1144/pygs.49.2.105.

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8

Okrusch, Martin, and Hans Ulrich Bambauer. "From the Fortschritte der Mineralogie to the European Journal of Mineralogy: a case history." European Journal of Mineralogy 22, no. 6 (December 23, 2010): 897–908. http://dx.doi.org/10.1127/0935-1221/2010/0022-2047.

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9

MATSUBARA, Satoshi. "Descriptive Mineralogy." Japanese Magazine of Mineralogical and Petrological Sciences 32, no. 3 (2003): 126–27. http://dx.doi.org/10.2465/gkk.32.126.

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10

Rakovan, John. "Environmental Mineralogy." Rocks & Minerals 83, no. 2 (March 2008): 172–75. http://dx.doi.org/10.3200/rmin.83.2.172-175.

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11

Kotova, O. B., and A. V. Ponaryadov. "Nanotechnological mineralogy." Journal of Mining Science 45, no. 1 (January 2009): 93–98. http://dx.doi.org/10.1007/s10913-009-0012-y.

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12

Bain, D. C. "Optical mineralogy." Earth-Science Reviews 24, no. 4 (October 1987): 284–85. http://dx.doi.org/10.1016/0012-8252(87)90068-7.

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13

Pernklau, Ernst. "Optical mineralogy." Chemical Geology 56, no. 3-4 (October 1986): 335. http://dx.doi.org/10.1016/0009-2541(86)90013-6.

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14

van Hullebusch, Eric, and Stephanie Rossano. "Mineralogy, environment and health." European Journal of Mineralogy 22, no. 5 (November 2, 2010): 627. http://dx.doi.org/10.1127/0935-1221/2010/0022-2064.

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15

Paykov, Oksana, and Harmonie Hawley. "Property-based assessment of soil mineralogy using mineralogy charts." Applied Clay Science 104 (February 2015): 261–68. http://dx.doi.org/10.1016/j.clay.2014.12.003.

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16

Artioli, Gilberto, and Ivana Angelini. "Mineralogy and archaeometry: fatal attraction." European Journal of Mineralogy 23, no. 6 (December 21, 2011): 849–55. http://dx.doi.org/10.1127/0935-1221/2011/0023-2119.

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17

Passaglia, Elio, and Ermanno Galli. "Natural zeolites: mineralogy and applications." European Journal of Mineralogy 3, no. 4 (August 27, 1991): 637–40. http://dx.doi.org/10.1127/ejm/3/4/0637.

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18

MURAKAMI, Takashi. "Reactions in mineralogy." Japanese Magazine of Mineralogical and Petrological Sciences 32, no. 3 (2003): 161–64. http://dx.doi.org/10.2465/gkk.32.161.

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19

SUGIYAMA, Kazumasa, and Akihiko NAKATSUKA. "Mineralogy and Crystallography." Nihon Kessho Gakkaishi 56, no. 3 (2014): 149. http://dx.doi.org/10.5940/jcrsj.56.149.

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20

Knittle, Elise. "Introduction to Mineralogy." Eos, Transactions American Geophysical Union 81, no. 34 (2000): 389. http://dx.doi.org/10.1029/00eo00292.

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21

Butcher, Alan R. "Applied Mineralogy ’03." Minerals Engineering 16, no. 6 (June 2003): 571. http://dx.doi.org/10.1016/s0892-6875(03)00144-4.

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22

Bloodworth, Andrew. "Mineralogy: Painful extractions." Nature 517, no. 7533 (January 2015): 142–43. http://dx.doi.org/10.1038/517142a.

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23

Vaughan, David J., and Claire L. Corkhill. "Mineralogy of Sulfides." Elements 13, no. 2 (April 1, 2017): 81–87. http://dx.doi.org/10.2113/gselements.13.2.81.

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24

TOKONAMI, Masayasu. "Applications for mineralogy." Hyomen Kagaku 7, no. 1 (1986): 117–20. http://dx.doi.org/10.1380/jsssj.7.117.

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25

Downs, James W. "Manual of mineralogy." Geochimica et Cosmochimica Acta 59, no. 9 (May 1995): 1901. http://dx.doi.org/10.1016/0016-7037(95)90150-7.

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26

Haggerty, Stephen E. "Upper mantle mineralogy." Journal of Geodynamics 20, no. 4 (December 1995): 331–64. http://dx.doi.org/10.1016/0264-3707(95)00016-3.

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27

Escolme, Angela, Ron F. Berry, Julie Hunt, Scott Halley, and Warren Potma. "Predictive Models of Mineralogy from Whole-Rock Assay Data: Case Study from the Productora Cu-Au-Mo Deposit, Chile." Economic Geology 114, no. 8 (December 1, 2019): 1513–42. http://dx.doi.org/10.5382/econgeo.2019.4650.

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Abstract Mineralogy is a fundamental characteristic of a given rock mass throughout the mining value chain. Understanding bulk mineralogy is critical when making predictions on processing performance. However, current methods for estimating complex bulk mineralogy are typically slow and expensive. Whole-rock geochemical data can be utilized to estimate bulk mineralogy using a combination of ternary diagrams and bivariate plots to classify alteration assemblages (alteration mapping), a qualitative approach, or through calculated mineralogy, a predictive quantitative approach. Both these techniques were tested using a data set of multielement geochemistry and mineralogy measured by semiquantitative X-ray diffraction data from the Productora Cu-Au-Mo deposit, Chile. Using geochemistry, samples from Productora were classified into populations based on their dominant alteration assemblage, including quartz-rich, Fe oxide, sodic, potassic, muscovite (sericite)- and clay-alteration, and least altered populations. Samples were also classified by their dominant sulfide mineralogy. Results indicate that alteration mapping through a range of graphical plots provides a rapid and simple appraisal of dominant mineral assemblage, which closely matches the measured mineralogy. In this study, calculated mineralogy using linear programming was also used to generate robust quantitative estimates for major mineral phases, including quartz and total feldspars as well as pyrite, iron oxides, chalcopyrite, and molybdenite, which matched the measured mineralogy data extremely well (R2 values greater than 0.78, low to moderate root mean square error). The results demonstrate that calculated mineralogy can be applied in the mining environment to significantly increase bulk mineralogy data and quantitatively map mineralogical variability. This was useful even though several minerals were challenging to model due to compositional similarities and clays and carbonates could not be predicted accurately.

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28

Dunham, A. C. "Developments in industrial mineralogy: I. The mineralogy of brick-making." Proceedings of the Yorkshire Geological Society 49, no. 2 (November 1992): 95–104. http://dx.doi.org/10.1144/pygs.49.2.95.

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29

Fang, Qian, Hanlie Hong, Lulu Zhao, Stephanie Kukolich, Ke Yin, and Chaowen Wang. "Visible and Near-Infrared Reflectance Spectroscopy for Investigating Soil Mineralogy: A Review." Journal of Spectroscopy 2018 (2018): 1–14. http://dx.doi.org/10.1155/2018/3168974.

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Clay minerals are the most reactive and important inorganic components in soils, but soil mineralogy classifies as a minor topic in soil sciences. Revisiting soil mineralogy has been gradually required. Clay minerals in soils are more complex and less well crystallized than those in sedimentary rocks, and thus, they display more complicated X-ray diffraction (XRD) patterns. Traditional characterization methods such as XRD are usually expensive and time-consuming, and they are therefore inappropriate for large datasets, whereas visible and near-infrared reflectance spectroscopy (VNIR) is a quick, cost-efficient, and nondestructive technique for analyzing soil mineralogic properties of large datasets. The main objectives of this review are to bring readers up to date with information and understanding of VNIR as it relates to soil mineralogy and attracts more attention from a wide variety of readers to revisit soil mineralogy. We begin our review with a description of fundamentals of VNIR. We then review common methods to process soil VNIR spectra and summary spectral features of soil minerals with particular attention to those <2 μm fractions. We further critically review applications of chemometric methods and related model building in spectroscopic soil mineral studies. We then compare spectral measurement with multivariate calibration methods, and we suggest that they both produce excellent results depending on the situation. Finally, we suggest a few avenues of future research, including the development of theoretical calibrations of VNIR more suitable for various soil samples worldwide, better elucidation of clay mineral-soil organic carbon (SOC) interactions, and building the concept of integrated soil mapping through combined information (e.g., mineral composition, soil organic matter-SOM, SOC, pH, and moisture).

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30

Shchiptsov, V. V. "Technological mineralogy: from Academician V. M. Severgin to the present day." Vestnik of Geosciences 4 (2021): 20–24. http://dx.doi.org/10.19110/geov.2021.4.3.

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It is shown that the origins of technological mineralogy in Russia are associated with the name of Academician V. M. Severgin, who at the end of the 18th century introduced the concept of «technological and economic» mineralogy. The stage of development of 1921—1955 is considered as important for the formation of the school of applied mineralogy. The next stage is the implementation of the principles of technological mineralogy in the practice of geological exploration and mining production and the creation of the Technological Mineralogy Commission of the All-Union Mineralogical Society by the beginning of 1983. The main directions of the development of technological mineralogy and the role of the published works of the commission are substantiated.

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31

Burns, Roger G. "Spectroscopic Methods in Mineralogy and Geology reviews in mineralogy, vol. 18." Geochimica et Cosmochimica Acta 54, no. 1 (January 1990): 253. http://dx.doi.org/10.1016/0016-7037(90)90214-6.

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32

Jones, Anthony P. "The mineralogy of cosmic dust: astromineralogy." European Journal of Mineralogy 19, no. 6 (December 17, 2007): 771–82. http://dx.doi.org/10.1127/0935-1221/2007/0019-1766.

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33

Keulen, Nynke, Sebastian Næsby Malkki, and Shaun Graham. "Automated Quantitative Mineralogy Applied to Metamorphic Rocks." Minerals 10, no. 1 (January 3, 2020): 47. http://dx.doi.org/10.3390/min10010047.

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The ability to apply automated quantitative mineralogy (AQM) on metamorphic rocks was investigated on samples from the Fiskenæsset complex, Greenland. AQM provides the possibility to visualize and quantify microstructures, minerals, as well as the morphology and chemistry of the investigated samples. Here, we applied the ZEISS Mineralogic software platform as an AQM tool, which has integrated matrix corrections and full quantification of energy dispersive spectrometry data, and therefore is able to give detailed chemical information on each pixel in the AQM mineral maps. This has been applied to create mineral maps, element concentration maps, element ratio maps, mineral association maps, as well as to morphochemically classify individual minerals for their grain shape, size, and orientation. The visualization of metamorphic textures, while at the same time quantifying their textures, is the great strength of AQM and is an ideal tool to lift microscopy from the qualitative to the quantitative level.

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34

Gunter, Mickey Eugene, and Stephen Matthew Schares. "Computerized Optical Mineralogy Calculations." Journal of Geological Education 39, no. 4 (September 1991): 289–90. http://dx.doi.org/10.5408/0022-1368-39.4.289.

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35

NAKAI, Izumi. "Inorganic Materials and Mineralogy." Journal of the Mineralogical Society of Japan 18, no. 6 (1989): 369–81. http://dx.doi.org/10.2465/gkk1952.18.369.

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36

Artioli, Gilberto. "Mineralogy and Cultural Heritage." CHIMIA International Journal for Chemistry 64, no. 10 (October 29, 2010): 712–15. http://dx.doi.org/10.2533/chimia.2010.712.

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37

Journet, Emilie. "A matter of mineralogy." Nature Geoscience 2, no. 5 (May 2009): 317–18. http://dx.doi.org/10.1038/ngeo512.

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38

KIMURA, Makoto. "Introduction to Meteorite Mineralogy." Japanese Magazine of Mineralogical and Petrological Sciences 44, no. 1 (2015): 1–9. http://dx.doi.org/10.2465/gkk.141210.

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39

MIZOTA, Tadato. "Mineralogy and material sciences." Japanese Magazine of Mineralogical and Petrological Sciences 32, no. 3 (2003): 152–56. http://dx.doi.org/10.2465/gkk.32.152.

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40

de Fourestier, Jeffrey. "China, Chinese, and mineralogy." Rocks & Minerals 80, no. 2 (March 2005): 118–24. http://dx.doi.org/10.3200/rmin.80.2.118-124.

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41

Villa, Igor M., and John M. Hanchar. "Age discordance and mineralogy." American Mineralogist 102, no. 12 (December 1, 2017): 2422–39. http://dx.doi.org/10.2138/am-2017-6084.

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42

Burns, Roger G. "Absorption spectroscopy in mineralogy." Geochimica et Cosmochimica Acta 55, no. 4 (April 1991): 1200. http://dx.doi.org/10.1016/0016-7037(91)90181-4.

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43

Namdar, A. "Mineralogy in Geotechnical Engineering." Journal of Engineering Science and Technology Review 3, no. 1 (June 2010): 108–10. http://dx.doi.org/10.25103/jestr.031.18.

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44

Wills, B. A. "Mineralogy tutorials-CD-ROM." Minerals Engineering 9, no. 5 (May 1996): 592. http://dx.doi.org/10.1016/s0892-6875(96)90028-x.

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45

Duffy, Thomas S. "Mineralogy at the extremes." Nature 451, no. 7176 (January 2008): 269–70. http://dx.doi.org/10.1038/nature06584.

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46

Skinner, H. Catherine W. "Mineralogy of Asbestos Minerals." Indoor and Built Environment 12, no. 6 (December 2003): 385–89. http://dx.doi.org/10.1177/1420326x03037003.

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47

Burbine, Thomas H., and Richard P. Binzel. "Asteroid Spectroscopy and Mineralogy." Symposium - International Astronomical Union 160 (1994): 255–70. http://dx.doi.org/10.1017/s0074180900046581.

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Spectroscopic observations of asteroids of smaller sizes and in the near-infrared have led to many exciting discoveries that have increased substantially our knowledge of the mineralogy of asteroids. These discoveries include the identification of hydrated M and E-asteroids, the mineralogical diversity of the S-class, anomalous S-asteroids, a possible source body of the aubrites, Vesta-like objects in the main belt, possible ordinary chondrite-like objects and one of the reddest objects in the solar system.

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48

A.M., Askhabov, and Kotova O.B. "Horizons of applied mineralogy." Zapiski RMO (Proceedings of the Russian Mineralogical Society) 148, no. 6 (2019): 117–25. http://dx.doi.org/10.30695/zrmo/2019.1486.06.

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49

Akbarzadeh, Daryoosh, Fariba Sharifian, and Azadeh Heidar Pour. "Mineralogy of Sasanian Bullae." Parseh Journal of Archaeological Studies 3, no. 9 (December 1, 2019): 139–46. http://dx.doi.org/10.30699/pjas.3.9.139.

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50

Dilles, John. "Sulfide Mineralogy and Geochemistry." Eos, Transactions American Geophysical Union 88, no. 9 (February 27, 2007): 112. http://dx.doi.org/10.1029/2007eo090013.

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